Net primary production in the Gulf Stream sustained by quasi-geostrophic vertical exchanges
© 2015. American Geophysical Union. All Rights Reserved. We analyze 12-years of mesoscale vertical motion derived from an observation-based product in the top 1000-m of the North West Atlantic Ocean. Vertical velocities (O(10-m-d-1)) associated with Gulf Stream instabilities consist of alternating c...
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ftcsic:oai:digital.csic.es:10261/123146 2024-02-11T10:06:57+01:00 Net primary production in the Gulf Stream sustained by quasi-geostrophic vertical exchanges Pascual, Ananda Ruiz, Simón Buongiorno Nardelli, Bruno Guinehut, Stephanie Iudicone, Daniele Tintoré, Joaquín European Commission Ministerio de Economía y Competitividad (España) 2015-01-28 http://hdl.handle.net/10261/123146 https://doi.org/10.1002/2014GL062569 https://doi.org/10.13039/501100000780 https://doi.org/10.13039/501100003329 unknown American Geophysical Union #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/EC/FP7/218812 Publisher's version http://dx.doi.org/10.1002/2014GL062569 Sí doi:10.1002/2014GL062569 issn: 1944-8007 Geophysical Research Letters 42(2): 441-449 (2015) http://hdl.handle.net/10261/123146 http://dx.doi.org/10.13039/501100000780 http://dx.doi.org/10.13039/501100003329 open Argo mesoscale vertical velocity primary production quasi-geostrophic dynamics artículo http://purl.org/coar/resource_type/c_6501 2015 ftcsic https://doi.org/10.1002/2014GL06256910.13039/50110000078010.13039/501100003329 2024-01-16T10:11:03Z © 2015. American Geophysical Union. All Rights Reserved. We analyze 12-years of mesoscale vertical motion derived from an observation-based product in the top 1000-m of the North West Atlantic Ocean. Vertical velocities (O(10-m-d-1)) associated with Gulf Stream instabilities consist of alternating cells of upwelling and downwelling. Here we show that the magnitude of the vertical motions decays exponentially southward with an e-folding length scale that is informative on the dynamics of the system. We further investigate the impact of the vertical supply of nutrients about phytoplankton growth with a conceptual model incorporating the mean effect of nutrient distribution, quasi-geostrophic dynamics, and Ekman suction/pumping. Results confirm that the mean effect of mesoscale vertical velocity variability alone can sustain observed levels of net primary production in the immediate vicinity of the Gulf Stream, while other mechanisms, including horizontal advection and submesoscale dynamics, need to be considered when moving toward the subtropical gyre. This work has been carried out as part of MESCLA (PB-LC 10–013) and E-MOTION (CTM2012-31014) projects, funded within the Open Call for R&D activities in the framework the MyOcean project (EU FP7-SPACE-2007-1-grant agreement 218812) and the Spanish National Research Program, respectively Peer Reviewed Article in Journal/Newspaper North West Atlantic Digital.CSIC (Spanish National Research Council) Geophysical Research Letters 42 2 441 449 |
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Open Polar |
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Digital.CSIC (Spanish National Research Council) |
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ftcsic |
language |
unknown |
topic |
Argo mesoscale vertical velocity primary production quasi-geostrophic dynamics |
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Argo mesoscale vertical velocity primary production quasi-geostrophic dynamics Pascual, Ananda Ruiz, Simón Buongiorno Nardelli, Bruno Guinehut, Stephanie Iudicone, Daniele Tintoré, Joaquín Net primary production in the Gulf Stream sustained by quasi-geostrophic vertical exchanges |
topic_facet |
Argo mesoscale vertical velocity primary production quasi-geostrophic dynamics |
description |
© 2015. American Geophysical Union. All Rights Reserved. We analyze 12-years of mesoscale vertical motion derived from an observation-based product in the top 1000-m of the North West Atlantic Ocean. Vertical velocities (O(10-m-d-1)) associated with Gulf Stream instabilities consist of alternating cells of upwelling and downwelling. Here we show that the magnitude of the vertical motions decays exponentially southward with an e-folding length scale that is informative on the dynamics of the system. We further investigate the impact of the vertical supply of nutrients about phytoplankton growth with a conceptual model incorporating the mean effect of nutrient distribution, quasi-geostrophic dynamics, and Ekman suction/pumping. Results confirm that the mean effect of mesoscale vertical velocity variability alone can sustain observed levels of net primary production in the immediate vicinity of the Gulf Stream, while other mechanisms, including horizontal advection and submesoscale dynamics, need to be considered when moving toward the subtropical gyre. This work has been carried out as part of MESCLA (PB-LC 10–013) and E-MOTION (CTM2012-31014) projects, funded within the Open Call for R&D activities in the framework the MyOcean project (EU FP7-SPACE-2007-1-grant agreement 218812) and the Spanish National Research Program, respectively Peer Reviewed |
author2 |
European Commission Ministerio de Economía y Competitividad (España) |
format |
Article in Journal/Newspaper |
author |
Pascual, Ananda Ruiz, Simón Buongiorno Nardelli, Bruno Guinehut, Stephanie Iudicone, Daniele Tintoré, Joaquín |
author_facet |
Pascual, Ananda Ruiz, Simón Buongiorno Nardelli, Bruno Guinehut, Stephanie Iudicone, Daniele Tintoré, Joaquín |
author_sort |
Pascual, Ananda |
title |
Net primary production in the Gulf Stream sustained by quasi-geostrophic vertical exchanges |
title_short |
Net primary production in the Gulf Stream sustained by quasi-geostrophic vertical exchanges |
title_full |
Net primary production in the Gulf Stream sustained by quasi-geostrophic vertical exchanges |
title_fullStr |
Net primary production in the Gulf Stream sustained by quasi-geostrophic vertical exchanges |
title_full_unstemmed |
Net primary production in the Gulf Stream sustained by quasi-geostrophic vertical exchanges |
title_sort |
net primary production in the gulf stream sustained by quasi-geostrophic vertical exchanges |
publisher |
American Geophysical Union |
publishDate |
2015 |
url |
http://hdl.handle.net/10261/123146 https://doi.org/10.1002/2014GL062569 https://doi.org/10.13039/501100000780 https://doi.org/10.13039/501100003329 |
genre |
North West Atlantic |
genre_facet |
North West Atlantic |
op_relation |
#PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/EC/FP7/218812 Publisher's version http://dx.doi.org/10.1002/2014GL062569 Sí doi:10.1002/2014GL062569 issn: 1944-8007 Geophysical Research Letters 42(2): 441-449 (2015) http://hdl.handle.net/10261/123146 http://dx.doi.org/10.13039/501100000780 http://dx.doi.org/10.13039/501100003329 |
op_rights |
open |
op_doi |
https://doi.org/10.1002/2014GL06256910.13039/50110000078010.13039/501100003329 |
container_title |
Geophysical Research Letters |
container_volume |
42 |
container_issue |
2 |
container_start_page |
441 |
op_container_end_page |
449 |
_version_ |
1790604994495381504 |